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25 results for “Priabonian”
Fig. 1 a-b in Large Benthic Foraminifera Pfendericonus Globulus Sirel & Deceviler In Sirel Et Al., 2020 (Priabonian Of Turkey): A Junior Synonym Of Pfendericonus Mindanaoensis Matsumaru, 2017 (Thanetian? Of The Philippine Archipelago)
Fig. 1 a-b Pfendericonus mindanaoensis (from Matsumaru, 2017, pl. 4, fig. 11, figured as Chrysalidina sp. and pl. 4, fig. 8, holotype specimen) of Selandian or Thanetian age from the Island of Mindanao, Philippine Archipelago. c-d Pfendericonus globulus Sirel & Deceviler (from Sirel et al., 2020, fig. 11I and 11J) from the Priabonian of NW Turkey.
Fig. 8 in Priabonian, late Eocene chronostratigraphy, depositional environment, and paleosol-trace fossil associations, Pipestone Springs, southwest Montana, USA
Fig. 8. Correlation of Pipestone Springs and Flagstaff Rim upper Eocene lithostratigraphy, and stratigraphic position of tuffs and vertebrate assemblages. → A. Location of Flagstaff Rim (Wyoming) and Pipestone Springs (Montana). B. Pipestone Springs reference section and Flagstaff Rim section showing its lithostratigraphy, and stratigraphic position of tuffs and vertebrate assemblages. Sections are correlated based upon Pipestone Spring's 40Ar/39Ar age of 36.00±0.20 Ma tuff and Flagstaff Rim's Ash B, and on middle Chadronian vertebrate assemblages in the PSMP and between Flagstaff Rim's Ash B to Ash G. 40Ar/39Ar age controls for Pipestone Springs strata are from this study; Flagstaff Rim tuff ages are from Swisher and Prothero (1990), Obradovich et al. (1995), and Sahy et al. (2015) Abbreviations: An, anorthoclase; Bi, biotite; S, sanidine (denote minerals used for single crystal 40Ar/39Ar age analyses of tuffs).
Fig. 4 - Palinurellusa bericus n in Palinurellus bericus n. sp. (Crustacea, Decapoda, Palinuridae) from the late Eocene (Priabonian) of San Feliciano (Orgiano, Vicenza, northeastern Italy)
Fig. 4 - Palinurellusa bericus n. sp., es. MSNM i28011, holotype / olotipo. A) Dorsal view / visione dorsale. B) Lateral view / visione laterale. Scale bar equal: 10 mm.
Fig. 2 in Palinurellus bericus n. sp. (Crustacea, Decapoda, Palinuridae) from the late Eocene (Priabonian) of San Feliciano (Orgiano, Vicenza, northeastern Italy)
Fig. 2 - Quarry at San Feliciano hill. / Cava di SAn Feliciano. A) Calcarenitic levels including corals and decapod crustaceans / visione dei livelli calcarenitici contenenti coralli e crostacei. B) Detail of one calcarenitc level with branched corals (Plocophyllia sp.) / dettaglio di un livello calcarenititco con colonia di coralli ramificati (Plocophyllia sp.). C) Calcarenitic level with coral in section (Plocophyllia sp.) / livello calcarenitico con sezioni di coralli (Plocophyllia sp.).
Fig. 3 - A in Palinurellus bericus n. sp. (Crustacea, Decapoda, Palinuridae) from the late Eocene (Priabonian) of San Feliciano (Orgiano, Vicenza, northeastern Italy)
Fig. 3 - A) Palinurellus bericus n. sp., reconstruction of the carapace/ Palinurellusa bericus n. sp., ricostruzione del carapace. B) Palinurellus wieneckii (De Man, 1881) (after Holthuis, 1991).
Fig. 1 in Palinurellus bericus n. sp. (Crustacea, Decapoda, Palinuridae) from the late Eocene (Priabonian) of San Feliciano (Orgiano, Vicenza, northeastern Italy)
Fig. 1 - Berici Mounts with location of the fossiliferous site. / Mappa dei Monti Berici con localizzazione della località fossilifera.
Text-fig. 5. Free living colonies, showing a mode of preservation which does not allow for precise determination but clearly exhibiting features characteristic for Smittipora and/or Cupuladria and/or Reusirella. (note the clear intrazooecial buds). Specimen deposited in NM Prague under number T 3319. A – imprint, B – counterpart to fig A. C – Specimen deposited in SNM under number Z 37724. Optic photography. Scale bar 1 mm. in The Priabonian Bryozoan-Decapod Association From The Borové Formation (The Ďurkovec Quarry, Ne Slovakia) And Its Palaeoecological Implications
Text-fig. 5. Free living colonies, showing a mode of preservation which does not allow for precise determination but clearly exhibiting features characteristic for Smittipora and/or Cupuladria and/or Reusirella. (note the clear intrazooecial buds). Specimen deposited in NM Prague under number T 3319. A – imprint, B – counterpart to fig A. C – Specimen deposited in SNM under number Z 37724. Optic photography. Scale bar 1 mm.
Text-fig. 4. Reteporella sp., deposited in NM Prague under number T 3318. A – Large colony suggesting very short transport. Scale bar 10 mm. Optic photography. B – the detail of branch showing the mode of preservation (no original skeleton preserved). Scale bar 1 mm. SEM photography (BSE detector). in The Priabonian Bryozoan-Decapod Association From The Borové Formation (The Ďurkovec Quarry, Ne Slovakia) And Its Palaeoecological Implications
Text-fig. 4. Reteporella sp., deposited in NM Prague under number T 3318. A – Large colony suggesting very short transport. Scale bar 10 mm. Optic photography. B – the detail of branch showing the mode of preservation (no original skeleton preserved). Scale bar 1 mm. SEM photography (BSE detector).
Text-fig. 7. rigid erect bryozoans. A – colony perhaps belonging to Metrarabdotos and/or Smittina, deposited in NM Prague under number T 3321. B – erect rigid cyclostomatous bryozoans belonging perhaps to the genus Hornera, deposited in NM Prague under number T 3322. C – colony perhaps belonging to Myriapora, deposited in NM Prague under number T 3323. All photographs were taken under the optic microscope, all scale bars 1 mm. in The Priabonian Bryozoan-Decapod Association From The Borové Formation (The Ďurkovec Quarry, Ne Slovakia) And Its Palaeoecological Implications
Text-fig. 7. rigid erect bryozoans. A – colony perhaps belonging to Metrarabdotos and/or Smittina, deposited in NM Prague under number T 3321. B – erect rigid cyclostomatous bryozoans belonging perhaps to the genus Hornera, deposited in NM Prague under number T 3322. C – colony perhaps belonging to Myriapora, deposited in NM Prague under number T 3323. All photographs were taken under the optic microscope, all scale bars 1 mm.
Text-fig. 6. Lunulites(?), deposited in NM Prague under number T 3320. A – optic (scale bar 1 mm) and B – SEM (BSE detector) photography (scale bar 100 µm) showing characters suggesting determination as Lunulites (square shape and linear arrangement of autozooecia, short cryptocyst and presence of vibracularia). in The Priabonian Bryozoan-Decapod Association From The Borové Formation (The Ďurkovec Quarry, Ne Slovakia) And Its Palaeoecological Implications
Text-fig. 6. Lunulites(?), deposited in NM Prague under number T 3320. A – optic (scale bar 1 mm) and B – SEM (BSE detector) photography (scale bar 100 µm) showing characters suggesting determination as Lunulites (square shape and linear arrangement of autozooecia, short cryptocyst and presence of vibracularia).
Text-fig. 3. Coeloma vigil A. MILNE-EDWARDS. Nearly complete specimens from several different layers. A – layer 15; B – layer 11; C – layer 16. All specimens are deposited at KGP MH. Key: ch=chelipeds; es=eye stalks; p=pereiopods. Scale bar 10 mm. Specimens were covered with ammonium chloride prior to photography. in The Priabonian Bryozoan-Decapod Association From The Borové Formation (The Ďurkovec Quarry, Ne Slovakia) And Its Palaeoecological Implications
Text-fig. 3. Coeloma vigil A. MILNE-EDWARDS. Nearly complete specimens from several different layers. A – layer 15; B – layer 11; C – layer 16. All specimens are deposited at KGP MH. Key: ch=chelipeds; es=eye stalks; p=pereiopods. Scale bar 10 mm. Specimens were covered with ammonium chloride prior to photography.
Figure 1 in Thallisellites augustinusii sp. nov. (Coleoptera: Erotylidae: Languriinae) from Priabonian Baltic amber
Figure 1. Thallisellites augustinusii Lyubarsky et Perkovsky sp. nov.: 1A – head, frontal view; 1B – antennae; 1C – general view, dorsally.
Figure 2 in Thallisellites augustinusii sp. nov. (Coleoptera: Erotylidae: Languriinae) from Priabonian Baltic amber
Figure 2. Thallisellites augustinusii Lyubarsky et Perkovsky sp. nov.: 2A – dorsolateral view; 2B – ventral view; 2C – lateral view.
Fig. 15. Priabonian Heterostegina from different Western Tethyan localities. A–C in The middle to late Eocene evolution of nummulitid foraminifer Heterostegina in the Western Tethys
Fig. 15. Priabonian Heterostegina from different Western Tethyan localities. A–C. Heterostegina reticulata mossanensis ssp. nov., earliest Priabonian, SBZ 19 A. A. Verona (N Italy), Castel San Felice, hairpin bend: MÁFI E. 9565, A−form, equatorial section. B, C: Mossano 7 (N Italy), A−form, equatorial sections, MÁFI E. 9566 (B), MÁFI E. 9567 (C). D–K. Heterostegina reticulata italica Herb, 1978. D, H. Mossano 8 (N Italy), late early Priabonian, SBZ 19 B, A−form, equatorial sections, MÁFI E. 9568 (D), MÁFI E. 9569 (H). E–G, I. Noszvaj (Hungary), "middle" Priabonian, SBZ 19/20. E–G. A−form, equatorial sections, MÁFI E. 9570 (E), MÁFI E. 9571 (F), MÁFI E. 9494 (G). I. MÁFI E. 9572, external view. J, K. Possagno 1 (NE Italy), late Priabonian, Ą
Fig. 14. Latest Bartonian and early Priabonian Heterostegina from different Western Tethyan localities. A–F in The middle to late Eocene evolution of nummulitid foraminifer Heterostegina in the Western Tethys
Fig. 14. Latest Bartonian and early Priabonian Heterostegina from different Western Tethyan localities. A–F. Heterostegina reticulata reticulata Rütimeyer, 1850, latest Bartonian, SBZ 18 C. A–E. Mossano 3 (N Italy), equatorial sections, MÁFI E. 9549, A−form (A), MÁFI E. 9550, A−form (B), MÁFI E. 9551, A−form (C), MÁFI E. 9552, B−form (D), MÁFI E. 9553, A−form (E). F. Vedi (Armenia), MÁFI E. 9554, A−form, equatorial section. G–R. Heterostegina reticulata mossanensis ssp. nov., earliest Priabonian, SBZ 19 A. G–J. Mossano 6, equatorial sections, holotype, MÁFI E. 9555, A−form (G), paratype, MÁFI E. 9556, A−form (H), paratype, MÁFI E. 9557, A−form (I), paratype, MÁFI E. 9558 (J), B−form. K–M. Úrhida 10 (Hungary), Ą
Figure 5 in Late Eocene (Priabonian) elasmobranchs from the Dry Branch Formation (Barnwell Group) of Aiken County, South Carolina, USA
Figure 5. Scyliorhinid shark teeth from the Dry Branch Formation (Priabonian) of Aiken County, South Carolina. A–G. Foumtizia sp. Anterior tooth in labial (A), lingual (B) and profile (C) views, SC2013.38. 27. Anterior tooth in labial (D) view, SC96.97.5. Anterior tooth in labial (E) view, SC96.97.6. Anterior tooth in labial view (F), SC96.97.7. Anterior tooth in labial view (G), SC 96.97.8. H–N. Premontreia (Oxyscyllium) sp. cf. Pr. (O.) gilberti. Anterior tooth in labial (H) and distal (I) views, SC2013.38.29. Labial at left in I. Anterior? tooth in labial (J), lingual (K) and basal (L) views, SC2013.38.30. Lateral tooth in labial (M) and lingual (N) views, SC2013.38.31. O–CC. Scyliorhinus sp. Lateral tooth in labial (O), lingual (P), occlusal (Q), and basal (R) views, SC2013.38.36. Anterolateral tooth in basal (S) view, SC2013.38.35. Lateral tooth in labial (T), lingual (U), and occlusal (V) views, SC2013.38.39. Lateral tooth in labial (W), lingual (X), and occlusal (Y) views, SC2013.38.37. Lateral tooth in labial (Z), lingual (AA), and occlusal (BB) views, SC2013.38.38. Anterior? tooth in occlusal (CC) view, SC2013.38.40. Labial at top in L, R, S; at bottom in Q, V, Y, BB, CC. Scale bars=1mm.
Figure 1. A in Late Eocene (Priabonian) elasmobranchs from the Dry Branch Formation (Barnwell Group) of Aiken County, South Carolina, USA
Figure 1. A. Outline map of southeastern US coastal states showing South Carolina, Aiken County (shaded region), and the city of Aiken. B. Generalized stratigraphic section of Barnwell Group strata in the Aiken, South Carolina area. The fossiliferous horizon at the South Aiken Site occurs approximately 2 m below the base of the Tobacco Road Formation. A and B modified from Cicimurri and Ebersole (2015). Abbreviations: NP=calcareous nannoplankton zone, O'burg=Orangeburg.
Figure 2 in Late Eocene (Priabonian) elasmobranchs from the Dry Branch Formation (Barnwell Group) of Aiken County, South Carolina, USA
Figure 2. Shark teeth from the Dry Branch Formation (Priabonian) of Aiken County, South Carolina. A–D. Notorynchus sp. cf. No. kempi teeth. Lower left tooth in lingual (A) and labial (B) views, SC2013.38.1. Lower right tooth in labial (C) and lingual (D) views, SC96.97.4. E. Squatina sp. cf. Sq. prima. Antero-lateral tooth in labial view, SC96.97.9. F, G. Nebrius sp. cf. Neb. thielensi. Anterolateral tooth in labial (F) and occlusal (G) views, SC2013.38.5. Labial at top in G. H. Ginglymostomatidae. Tooth in labial view, SC2013.38.7. I–O. Carcharias sp. Third lower right anterior tooth in labial (I) view, SC2001.1.55. Third upper right anterior tooth in lingual (J) and labial (K) views, SC2001.1.57. First lower right anterior tooth in labial (L) view, SC2001.1.59. Second lower right anterior tooth in labial (M) view, SC96.97.44.1. Second upper right anterior tooth in lingual (N) view, SC96.97.42. Lower left lateral tooth in lingual (O) view, SC96.97.43. P–S. Alopias sp. Tooth in labial (P) and lingual (Q) views, SC2001.1.65. Tooth in labial (R) and lingual (S) views, SC2001.1.66. Scale bars=1 cm in A–D, I–K, N, O; 5 mm in E–G, L–M, P–S; 1 mm in H.
Figure 7 in Late Eocene (Priabonian) elasmobranchs from the Dry Branch Formation (Barnwell Group) of Aiken County, South Carolina, USA
Figure 7. Myliobatidae teeth from the Dry Branch Formation (Priabonian) of Aiken County, South Carolina. A–E. Aetomylaeus sp. Incomplete lower median tooth in labial (A), lingual (B), and occlusal (C) and views, SC2001.1.2. Lateral tooth in occlusal (D) and profile (E) views, SC2001.1.29. F–I. Pseudaetobatus undulatus. Upper median tooth in occlusal (F) view, SC2013.38.86. Lower median tooth in occlusal (G) view, SC2013.38.84. Upper right distal-most lateral tooth in occlusal (H) and labial (I) views, SC2013.38.91. Lateral tooth in occlusal (J) view, SC2013.38.96.2. K–R. Rhinoptera sp. Lateral tooth in labial (K), lingual (L), occlusal (M), and basal (N) views, SC2001.1.12. Median tooth in occlusal (O), lingual (P), and basal (Q) views, SC2001.1.16. Lateral tooth in lingual (R) view, SC2013.38.70. Labial at top in C, D, F–H, J, M–O, Q; at right in E. Scale bars=1 cm in A–C, F–I, K–R; 5 mm in D, E, J.
Figure 4 in Late Eocene (Priabonian) elasmobranchs from the Dry Branch Formation (Barnwell Group) of Aiken County, South Carolina, USA
Figure 4. Carcharhiniform shark teeth from the Dry Branch Formation (Priabonian) of Aiken County, South Carolina. A–D. Carcharhinidae indeterminate. Anterolateral tooth in labial (A) and lingual (B) views, SC2013.38.105. Anterolateral tooth in labial (C) and lingual (D) views, SC2001.1.43. Labial at right in C. E–P. Isogomphodon aikenensis n. sp. Upper anterior tooth in lingual view (E), SC2013.38.110 (Holotype). Lower lateral tooth in labial (F) and lingual (G) views, SC2013.38.123.1. Lower anterior tooth in labial (H) and lingual (I) views, SC2013.38.119 (Paratype). Upper lateral tooth in labial (J) and lingual (K) views, SC2013.38.112 (Paratype). Posterolateral tooth in labial (L) and lingual (M) views, SC2013.38.114. Posterior tooth in labial (N) and lingual (O) views, SC2013.38.115 (Paratype). Upper anterolateral tooth in lingual (P) view, SC2013.38.111 (Paratype). Scale bars=1 cm in A–D; 5 mm in E–P.
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